Extraordinary Biomass-Burning Episode and Impact Winter Triggered by the Younger Dryas Cosmic Impact ∼12,800 Years Ago. 1. Ice Cores and Glaciers | The Journal of Geology: Ahead of Print

Extraordinary Biomass-Burning Episode and Impact Winter Triggered by the Younger Dryas Cosmic Impact ∼12,800 Years Ago. 1. Ice Cores and Glaciers | The Journal of Geology: Ahead of Print

Extraordinary Biomass-Burning Episode and Impact Winter Triggered by the Younger Dryas Cosmic Cosmic Impact 12800 Years Ago

Extraordinary Biomass-Burning Episode and Impact Winter Triggered by the Younger Dryas Cosmic Cosmic Impact 12800 Years Ago

The extent of Doggerland during the Younger Dryas, around 12,000 years ago

Caitlin R. Green - Suggested reindeer migration routes and the extent of Doggerland during the Younger Dryas about years ago at the end of the last Glacial Period of the Ice Age.

(Phys.org) —A period of rapid, intense cooling, known as the Younger Dryas, took place about 13,000 years ago. Scientists think this sudden change in climate caused the extinction of many large mammals, such as the mammoth, and was the reason for the disappearance of North America's Clovis people. According to one hypothesis, a cosmic impact caused the climate to cool. Using data from the Greenland ice core, Michail Petaev and his colleagues at Harvard University have found what appears to…

Younger Dryas climate anomalies in Greenland, the Cariaco Basin, Antarctica and freshwater forcing

RealClimate: Revisiting the Younger Dryas

Younger Dryas, North Atlantic circulation, MOC, abrupt climate change, last glacial maximum

Where did the water go?                                                                                                                                                                                 More

Evaporation, not outflow, drained ancient Lake Agassiz during the Younger Dryas

Yet another Younger Dryas impact paper | Musings on Quantitative Palaeoecology

Yet another Younger Dryas impact paper

Yet another Younger Dryas impact paper | Musings on Quantitative Palaeoecology

Evidence for an extraterrestrial impact 12,900 years ago that contributed to the megafaunal extinctions and the Younger Dryas cooling

Evidence for an extraterrestrial impact years ago that contributed to the megafaunal extinctions and the Younger Dryas cooling

Evaporation, not outflow, drained ancient Lake Agassiz during the Younger Dryas | Watts Up With That?

Evaporation, not outflow, drained ancient Lake Agassiz during the Younger Dryas

younger_dryas_graph

Younger Dryas climate event solved via nanodiamonds – it was a planetary impact event

Younger Dryas-- is a geological period from 12,900 to 11,700 calendar years ago (BP). It is named after an indicator genus, the alpine-tundra wildflower Dryas octopetala. Leaves of Dryas octopetala are occasionally abundant in the Late Glacial, often minerogenic-rich, lake sediments of Scandinavian lakes. Younger Dryas saw a sharp decline in temperature over most of the northern hemisphere, at the end of the Pleistocene epoch, immediately preceding the current warmer Holocene

Gazelle fossils in Israel indicate southern Levant not as dry during Younger Dryas as thought

Temporal Correlations between Lake Agassiz, the Okefenokee Swamp, and Ancient Flood Myths

Temporal Correlations between Lake Agassiz, the Okefenokee Swamp, and Ancient Flood Myths

Evaporation, not outflow, drained ancient Lake Agassiz during the Younger Dryas

Frontiers of Anthropology: Younger Dryas-Sudden Cooling

This reconstructed temperature map for the younger dryas event is more significant than the makers realised. It is also virtually a sna.

Younger Dryas event after a arctic/alpine flower Dryas Octopetald which had returned to Britain during this period, 12,800-11,500 years ago.

Younger Dryas event after a arctic/alpine flower Dryas Octopetald which had returned to Britain during this period, years ago.

Hunter-Gatherer Behavior: Human Response During The Younger Dryas PDF

Hunter-Gatherer Behavior: Human Response During The Younger Dryas PDF

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